Hydrogeochemical characterization of the areas of exploitation of the CBG sites: cas of the plateaus of N'Dangara and Boundou Wandé, Sous-préfecture de Sangarédi, Prefecture of Boké, Republic of Guinea

Y. Diallo, A. Konaté
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Abstract

Abstract This work aims to analyze the quality of groundwater in the riparian areas of the bauxitic plateaus of N'Dangara and Boundou Wandé in operation by the CBG (Compagnie des Bauxites de Guinée). The geology of the study area consists mainly of sedimentary formations of the Devonian faro, Neogene and Quaternary. Three water measurement and sampling campaigns on the two plateaus were carried out with determination of piezometric measurements and physic-chemical parameters. This study showed that the general flow direction of groundwater is dispersed. The flows at Boundou Wandé are from the center of the plateau to the north and that at N'Dangara is from the center to the south and southwest. It can be seen that the direction of groundwater flow reflects overall the relief of the deposit conditioned by its geomorphological framework. It emerges from the analysis of physical and chemical parameters that well water is consumable. However, the water from wells MW15, MW16, MW17, MW18 and MW21 with a low pH (4.84 to 5.13) may present a certain nuisance for its consumption and because it can be corrosive. Analysis of the Piper diagram showed two hydrogeochemical facies (calcium and magnesium bicarbonate facies and sodium and potassium carbonate facies). However, this study strongly suggests continuous monitoring of groundwater in and around the study area in order to meet the demand for water supply to communities without compromising the ability of future generations to meet water quality requirements.
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CBG场地开发区域的水文地球化学特征:几内亚共和国博凯州桑加雷迪省恩丹加拉和邦杜旺代高原的cas
摘要本工作旨在分析CBG (Compagnie des Bauxites de guinacei)运营的N'Dangara和Boundou wand铝土矿高原河岸地区的地下水质量。研究区地质主要为泥盆系法鲁、新近系和第四纪沉积组。在两个高原上进行了三次水测量和采样活动,并确定了压力测量和物理化学参数。研究表明,地下水总体流向是分散的。Boundou wand的水流是从高原中心向北流,而N'Dangara的水流是从高原中心向南和西南流。可以看出,地下水流动方向总体上反映了受地貌格局制约的沉积物起伏程度。通过对井水理化参数的分析可知,井水具有消耗性。然而,来自MW15、MW16、MW17、MW18和MW21井的水pH值较低(4.84至5.13),可能会对饮用造成一定的滋扰,因为它可能具有腐蚀性。Piper图分析显示两种水文地球化学相(碳酸氢钙镁相和碳酸钠钾相)。然而,本研究强烈建议对研究区内及其周围的地下水进行持续监测,以便在不影响后代满足水质要求的情况下满足社区供水需求。
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